Mark R. Frank, Ph.D.
Affiliations: | 2001 | University of Maryland, College Park, College Park, MD |
Area:
Geochemistry, GeologyGoogle:
"Mark Frank"Mean distance: (not calculated yet)
Parents
Sign in to add mentor| Philip A. Candela | grad student | 2001 | University of Maryland | |
| (An experimental investigation of ore metals in silicate melt -volatile phase systems.) | ||||
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Publications
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| Frank MR, Scott HP, Aarestad E, et al. (2016) Potassium chloride-bearing ice VII and ice planet dynamics Geochimica Et Cosmochimica Acta. 174: 156-166 |
| Fraley KJ, Frank MR. (2014) Gold solubilities in bornite, intermediate solid solution, and pyrrhotite at 500° to 700°C and 100 MPa Economic Geology. 109: 407-418 |
| Frank MR, Vaccaro DM. (2012) An experimental study of high temperature potassic alteration Geochimica Et Cosmochimica Acta. 83: 195-204 |
| Frank MR, Simon AC, Pettke T, et al. (2011) Gold and copper partitioning in magmatic-hydrothermal systems at 800°C and 100MPa Geochimica Et Cosmochimica Acta. 75: 2470-2482 |
| Fei Y, Ricolleau A, Frank M, et al. (2007) Toward an internally consistent pressure scale. Proceedings of the National Academy of Sciences of the United States of America. 104: 9182-6 |
| Candela PA, Crummett CD, Earnest DJ, et al. (2007) Low-pressure decomposition of chrysotile as a function of time and temperature American Mineralogist. 92: 1704-1713 |
| Simon AC, Frank MR, Pettke T, et al. (2007) An evaluation of synthetic fluid inclusions for the purpose of trapping equilibrated, coexisting, immiscible fluid phases at magmatic conditions American Mineralogist. 92: 124-138 |
| Simon AC, Frank MR, Pettke T, et al. (2005) Gold partitioning in melt-vapor-brine systems Geochimica Et Cosmochimica Acta. 69: 3321-3335 |
| Frank MR, Candela PA, Piccoli PM. (2003) Alkali exchange equilibria between a silicate melt and coexisting magmatic volatile phase: An experimental study at 800°C and 100 MPa Geochimica Et Cosmochimica Acta. 67: 1415-1427 |
| Frank MR, Candela PA, Piccoli PM. (1998) K-feldspar-muscovite-andalusite-quartz-brine phase equilibria: An experimental study at 25 to 60 MPa and 400 to 550°C Geochimica Et Cosmochimica Acta. 62: 3717-3727 |